• Study Resource
  • Explore Categories
    • Arts & Humanities
    • Business
    • Engineering & Technology
    • Foreign Language
    • History
    • Math
    • Science
    • Social Science

    Top subcategories

    • Advanced Math
    • Algebra
    • Basic Math
    • Calculus
    • Geometry
    • Linear Algebra
    • Pre-Algebra
    • Pre-Calculus
    • Statistics And Probability
    • Trigonometry
    • other →

    Top subcategories

    • Astronomy
    • Astrophysics
    • Biology
    • Chemistry
    • Earth Science
    • Environmental Science
    • Health Science
    • Physics
    • other →

    Top subcategories

    • Anthropology
    • Law
    • Political Science
    • Psychology
    • Sociology
    • other →

    Top subcategories

    • Accounting
    • Economics
    • Finance
    • Management
    • other →

    Top subcategories

    • Aerospace Engineering
    • Bioengineering
    • Chemical Engineering
    • Civil Engineering
    • Computer Science
    • Electrical Engineering
    • Industrial Engineering
    • Mechanical Engineering
    • Web Design
    • other →

    Top subcategories

    • Architecture
    • Communications
    • English
    • Gender Studies
    • Music
    • Performing Arts
    • Philosophy
    • Religious Studies
    • Writing
    • other →

    Top subcategories

    • Ancient History
    • European History
    • US History
    • World History
    • other →

    Top subcategories

    • Croatian
    • Czech
    • Finnish
    • Greek
    • Hindi
    • Japanese
    • Korean
    • Persian
    • Swedish
    • Turkish
    • other →
 
Profile Documents Logout
Upload
earthquakes - SCHOOLinSITES
earthquakes - SCHOOLinSITES

... P waves and S waves What are seismic waves that travel along earth’s surface called? Surface waves Waves that travel through solids liquids and gases are called P waves. P waves are the fastest waves, so they travel ahead of other seismic waves. What are P waves also called? Primary waves because th ...
Earthquakes
Earthquakes

...  Use instruments called seismographs  Record seismic waves  A drum with a sheet of paper vibrates and a stationary pen marks the vibrations on the paper  The height of the lines are used to measure the energy released from the earthquake called the magnitude ...
CHAPTER 12 EARTHQUAKES
CHAPTER 12 EARTHQUAKES

... speed of seismic waves increases abruptly at 30 km beneath the surface of continents. • Because the mantle is denser than the crust. • Therefore, this marks the boundary between the mantle and crust. • The depth of this boundary varies from 10 km under the oceans to 30 km under the continents. • Ear ...
Alfred Lothar Wegener, 1880-1930
Alfred Lothar Wegener, 1880-1930

... noticed the close fit between the coastlines of Africa and South America. Might the similarities among organisms be due, not to land bridges, but to the continents having been joined together at one time? As he later wrote: "A conviction of the fundamental soundness of the idea took root in my ...
Slide 1
Slide 1

... hot, it radiates a natural heat to the upper layers. • Because of this a current of heat comes into being. Those are also known as the convection currents. • The convection currents cause the movement of the tectonic plates. ...
~2.6 MB
~2.6 MB

... sub-slab trenchparallel flow of mantle material, and for a rapid reorientation of this flow at the northern edge of the Pacific plate. ...
What is an earthquake
What is an earthquake

... originates in a few rela-tively narrow zones that wind around the globe Major earthquake zones include the Circum-Pacific belt, Mediterranean Sea region to the Himalayan complex, and the ...
Earthquakes Unit STUDY GUIDE
Earthquakes Unit STUDY GUIDE

... a. near divergent boundaries. c. near transform boundaries. b. near convergent boundaries. d. along normal faults. The last seismic waves to arrive are a. P waves. c. surface waves. b. S waves. d. body waves. Strike-slip faults are prominent along ____ plate boundaries a. convergent c. transcontinen ...
pdf file - High Point University
pdf file - High Point University

... Figure 3: Top plate is positively charged and the bottom plate is negatively charged. Because the electric eld between the plates is constant, the electric potential varies linearly with y . Electric eld points from high potential to low potential. Therefore, the top plate is at a higher potential ...
Electron and Ion Dynamics of the Solar Wind Interaction with a
Electron and Ion Dynamics of the Solar Wind Interaction with a

... magnetic field lines drape around the nucleus. No bow shock develops, as expected for a weakly outgassing comet [22]. The heavy cometary ions are accelerated by the convective electric field, to be eventually picked up far downstream, whereas solar wind protons deflect in the opposite direction in a ...
Earthquakes
Earthquakes

...  P waves (primary waves)- longitudinal waves similar to sound waves  Move through solid and liquid material  Compress and expand the ground  Similar to an accordion or a slinky ...
Convection currents
Convection currents

... The movement of energy from a warmer object to a cooler object is called heat transfer. Heat is always transferred from a warmer substance to a cooler substance. There are three types of heat transfer: radiation, conduction, and convection. The transfer of energy through empty space is called radiat ...
Mechanical Waves
Mechanical Waves

... Sound is the movement of air particles created by a vibrating source. Air particles are in constant random motion, exerting very small pressure variations around the steady-state atmospheric pressure. Each particle is subject to both an inertial force (due to its mass and acceleration) and a force w ...
File - earth science online
File - earth science online

... Seismic Waves (cont.) Seismic waves – P waves • Travels through liquids as well as solids • In all materials, P waves travel faster than do S waves – S waves • Cannot travel through liquids Seismic Waves (cont.) Seismic waves – Seismic waves refract (bend) as they pass from one material to another – ...
What is an earthquake?
What is an earthquake?

... Locating an Earthquake  Earthquake ...
Science Grade 8 Daily PACT Review Questions
Science Grade 8 Daily PACT Review Questions

... common. Humans are also part of the most recent period of this era. The law of superposition states that each rock layer is older than the one above it. So using this layering, the relative age of the rock or fossil in the rock is older if it is farther down in the rock layers. Relative dating can b ...
Earth Science Regents Review
Earth Science Regents Review

... If the difference in arrival times of the P- and Swaves is 6 minutes 20 seconds, how far is the distance to the epicenter? ________________ A P-wave arrived at 3:32:00 p.m. and the S-wave arrived at 3:36:30 p.m. How far away is the ...
Field Notebook
Field Notebook

... What could influence the lag time between the arrival of S and P waves, other than distance from the epicenter? Claim: ...
Earthquakes - Fair Lawn Public Schools
Earthquakes - Fair Lawn Public Schools

... • 1. The Richter magnitude scale uses the amount of motion at a given distance from an earthquake to determine the magnitude of the earthquake. • 2. The moment magnitude scale measures the total amount of energy released by an earthquake. • 3. The Modified Mercalli scale measures the earthquake inte ...
Earth`s Interior Crust Mantle Core
Earth`s Interior Crust Mantle Core

... Mica Crystal with Quartz @ 5GPa ...
CompositionoftheEarth
CompositionoftheEarth

... A very wide range of temperatures are estimated for the outer core. They range from 2500℃ on the cooler end and 7500℃ on the hot side. The the movement of the outer core is thought to be responsible for the Magnetic field​ of the earth. Mantle The mantle is a little odd. It’s very hot but the rocks ...
Planetary Magnetic Fields: Achievements and Prospects
Planetary Magnetic Fields: Achievements and Prospects

... alloy, then an inner core will nucleate. In Earth, we know from seismic evidence that the core is ∼10% less dense than pure iron and many suggestions have been offered for the identity of the light elements that are mixed with the iron (Poirier 1994; Gessmann et al. 2001). As the inner core freezes, ...
Planetary Magnetic Fields: Achievements and Prospects
Planetary Magnetic Fields: Achievements and Prospects

... alloy, then an inner core will nucleate. In Earth, we know from seismic evidence that the core is ∼10% less dense than pure iron and many suggestions have been offered for the identity of the light elements that are mixed with the iron (Poirier 1994; Gessmann et al. 2001). As the inner core freezes, ...
Ch 7 Lesson 2 Outline
Ch 7 Lesson 2 Outline

... a. The direction of a magnetic field in minerals can be determined by using a device
 called a(n) ...
Earth`s vital statistics Shape: almost spherical almost spherical Size
Earth`s vital statistics Shape: almost spherical almost spherical Size

... •Waves are reflected or refracted according to the density of the material through which they travel •P waves are faster than S waves •There is a distinct S waves shadow zone •There is also a P wave shadow zone where they are significantly weaker •P waves appear on the other side of the earth, but a ...
< 1 ... 8 9 10 11 12 13 14 15 16 ... 35 >

Ionospheric dynamo region

In the height region between about 85 and 200 km altitude on Earth, the ionospheric plasma is electrically conducting. Atmospheric tidal winds due to differential solar heating or due to gravitational lunar forcing move the ionospheric plasma against the geomagnetic field lines thus generating electric fields and currents just like a dynamo coil moving against magnetic field lines. That region is therefore called ionospheric dynamo region. The magnetic manifestation of these electric currents on the ground can be observed during magnetospheric quiet conditions. They are called Sq-variations (S=solar; q=quiet) and L-variations (L=lunar) of the geomagnetic field.Additional electric currents are generated by the varying magnetospheric electric convection field. These are the DP1-currents (the auroral electrojets) and the polar DP2-currents. Finally, a polar-ring current has been derived from the observations which depends on the polarity of the interplanetary magnetic field. These geomagnetic variations belong to the so-called external part of the geomagnetic field. Their amplitudes reach at most about 1% of the main internal geomagnetic field Bo.
  • studyres.com © 2025
  • DMCA
  • Privacy
  • Terms
  • Report